Prior to this work, the planktic foraminiferal genus Beella Banner and Blow (1960) has never been described from Pleistocene sediments from the Norwegian-Greenland Sea (NGS). The general characteristics of this species agree well with the most recent emendation of the genus Beella. Accordingly, the described species is considered to be Beella megastoma (Earöamd). Test sizes range from 200-700 μm, but specimens are mainly confined to the 250-500 μm mesh-size fraction. Interpretations of stable isotopes, sedimentological, and other micropaleontological data indicate that this species is not simply a "warm-water form" and, despite its low abundances, it is a species of major paleoceanographic significance. Stratigraphically, it is confined to ...
Four long sediment cores from locations in the Framstrait, the Norwegian-Greenland Seas and the nort...
Paleoceanographic changes of surface water characteristics have been studied in the Nordic Seas duri...
Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacial...
Microfaunal studies of planktic foraminifera carried out on 21 sediment cores from the Norwegian-Gre...
International audienceAbstract Fluctuations in benthic foraminiferal faunas over the last 130,000 yr...
We present measurements of the maximum diameter of the planktonic foraminifer Neogloboquadrina pachy...
Turborotalita quinqueloba is a species of planktic foraminifera commonly found in the sub-polar Nort...
Fluctuations in benthic foraminiferal faunas over the last 130,000 yr in four piston cores from the ...
A high-resolution piston core, ENAM93-21, from a water depth of 1020 m near the Faeroe-Shetland Chan...
Foraminiferal assemblages were studied in northern Barents Sea core ASV 880 along with oxygen and ca...
Foraminiferal faunas were analysed from 22 cores (length 30-165 cm), three grab samples and one dred...
ABSTRACT: Deep-water agglutinated Foraminifera (DWAF) are investigated from Miocene sediments recove...
Benthic foraminifers were examined from Neogene sediments of Ocean Drilling Program (ODP) Sites 645,...
We present a record encompassing marine isotope stages 7-1 from a hitherto unexplored and heavily ic...
A multiproxy study of palaeoceanographic and climatic changes in northernmost Baffin Bay shows that ...
Four long sediment cores from locations in the Framstrait, the Norwegian-Greenland Seas and the nort...
Paleoceanographic changes of surface water characteristics have been studied in the Nordic Seas duri...
Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacial...
Microfaunal studies of planktic foraminifera carried out on 21 sediment cores from the Norwegian-Gre...
International audienceAbstract Fluctuations in benthic foraminiferal faunas over the last 130,000 yr...
We present measurements of the maximum diameter of the planktonic foraminifer Neogloboquadrina pachy...
Turborotalita quinqueloba is a species of planktic foraminifera commonly found in the sub-polar Nort...
Fluctuations in benthic foraminiferal faunas over the last 130,000 yr in four piston cores from the ...
A high-resolution piston core, ENAM93-21, from a water depth of 1020 m near the Faeroe-Shetland Chan...
Foraminiferal assemblages were studied in northern Barents Sea core ASV 880 along with oxygen and ca...
Foraminiferal faunas were analysed from 22 cores (length 30-165 cm), three grab samples and one dred...
ABSTRACT: Deep-water agglutinated Foraminifera (DWAF) are investigated from Miocene sediments recove...
Benthic foraminifers were examined from Neogene sediments of Ocean Drilling Program (ODP) Sites 645,...
We present a record encompassing marine isotope stages 7-1 from a hitherto unexplored and heavily ic...
A multiproxy study of palaeoceanographic and climatic changes in northernmost Baffin Bay shows that ...
Four long sediment cores from locations in the Framstrait, the Norwegian-Greenland Seas and the nort...
Paleoceanographic changes of surface water characteristics have been studied in the Nordic Seas duri...
Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacial...